The Kozani-Grevena (Greece) earthquake of May 13, 1995, a seismological study

Επιστημονική δημοσίευση - Άρθρο Περιοδικού uoadl:3018563 14 Αναγνώσεις

Μονάδα:
Ερευνητικό υλικό ΕΚΠΑ
Τίτλος:
The Kozani-Grevena (Greece) earthquake of May 13, 1995, a seismological study
Γλώσσες Τεκμηρίου:
Αγγλικά
Περίληψη:
We present a detailed seismological study of the Kozani earthquake. We relocate the mainshock with regional data at depth of 14.2 km beneath the Vourinos massif. We compute the focal mechanism by body waveform modeling at teleseismic distance and find a normal fault striking N240° and dipping 40° toward the NW with a centroid depth of 11 km. We installed a dense network of portable seismographs around the epicentral region and located several hundreds of aftershocks. The main cluster of aftershock seismicity defines a plane dipping north at an angle of about 35°, consistent with the main-shock mechanism, while some seismic activity is also seen on an antithetic fault. Our results suggest the active fault plane to be the Deskati fault which dips at a constant angle and therefore branches on the Paleohori fault where surface breaks were observed. We also compute 181 focal mechanisms which mostly show normal faulting.
Έτος δημοσίευσης:
1998
Συγγραφείς:
Hatzfeld, D.
Karakostas, V.
Ziazia, M.
Selvaggi, G.
Leborgne, S.
Berge, C.
Makropoulos, K.
Περιοδικό:
JOURNAL OF GEODYNAMICS
Τόμος:
26
Αριθμός / τεύχος:
2-4
Σελίδες:
245-254
Λέξεις-κλειδιά:
earthquake; focal mechanism, Greece, Macedonia, Kozani-Grevena
Επίσημο URL (Εκδότης):
DOI:
10.1016/S0264-3707(97)00063-X
Το ψηφιακό υλικό του τεκμηρίου δεν είναι διαθέσιμο.